{"id":42624,"date":"2023-10-26T06:46:56","date_gmt":"2023-10-26T06:46:56","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=42624"},"modified":"2023-10-26T06:50:57","modified_gmt":"2023-10-26T06:50:57","slug":"evolution-of-eastern-passive-margin-of-adria-recorded-in-shallow-to-deep%e2%80%91water-successions-of-the-transition-zone-between-the-alps-and-the-dinarides-ivanscica-mt-nw-croatia","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/evolution-of-eastern-passive-margin-of-adria-recorded-in-shallow-to-deep%e2%80%91water-successions-of-the-transition-zone-between-the-alps-and-the-dinarides-ivanscica-mt-nw-croatia\/","title":{"rendered":"Evolution of eastern passive margin of Adria recorded in shallow to deep\u2011water successions of the transition zone between the Alps and the Dinarides (Ivan\u0161\u010dica Mt., NW Croatia)"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_fullwidth_slider _builder_version=”4.16″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.16″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

NAJNOVIJI OBJAVLJENI RADOVI<\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.22.2″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Evolution of eastern passive margin of Adria recorded in shallow to deep<\/em><\/strong>\u2011water successions of the transition zone between the Alps and the Dinarides (Ivan\u0161\u010dica Mt., NW Croatia)<\/em><\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”20px||41px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ custom_padding=”0px|||||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/10\/facies.jpg” alt=”springer” title_text=”10347_68_1_oc_10347_67_3_OC” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.22.2″ width=”30%” max_width=”35%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px|||||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.22.2″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

U znanstvenom \u010dasopisu Facies objavljen je znanstveni rad pod naslovom Evolution of eastern passive margin of Adria recorded in shallow to deep<\/em><\/strong>\u2011water successions of the transition zone between the Alps and the Dinarides (Ivan\u0161\u010dica Mt., NW Croatia)<\/em><\/strong><\/p>\n

Rad je isklju\u010divo rezultat djelatnika Zavoda za Geologiju Hrvatskog geolo\u0161kog instituta.<\/p>\n

U radu su prikazani rezultati sedimentolo\u0161kih i paleontolo\u0161kih analiza kojima su prethodila detaljna i dugotrajna terenska istra\u017eivanja na podru\u010dju Ivan\u0161\u010dice u Hrvatskom zagorju. U ovom radu po prvi puta je detaljno snimljena i opisana gotovo kompletna jurska dubokovodna sedimentna sukcesija isto\u010dnog pasivnog kontinentalnog ruba Jadranske mikroplo\u010de. U sedimentnom zapisu mogu\u0107e je i\u0161\u010ditati jasne dokaze o dvama tektonskim impulsima koji su doveli do naglog produbljivanja talo\u017enog okoli\u0161a i uspostave neprekidne dubokovodne sedimentacije. Sedimentne stijene istog paleogeografskog podrijetla od ranije su bile poznate na podru\u010dju susjedne Bosne i Hercegovine, Slovenije, Austrije, ali ne i Hrvatske. Ovaj rad stoga donosi klju\u010dne spoznaje o evoluciji distalnog pasivnog ruba Jadranske mikroplo\u010de i tako popunjava prazninu na prijelazu Bosanskog bazena prema Slovenskom i Bledskom bazenu te Sjevernim Vapnena\u010dkim Alpama i precizira vrijeme tektonskih pokreta koji su doveli do formiranja sjeveroisto\u010dnog ruba Jadranske karbonatne platforme.<\/p>\n

Istra\u017eivanje je provedeno u okviru projekta Hrvatske zaklade za znanost \u201eVulkano-sedimentne sukcesije sjeverozapadne Hrvatske i njihova uloga u razumijevanju geodinamike Paleotetisa tijekom srednjeg Trijasa\u201c. Akronim GOST (IP-2019-04-3824), voditelj dr.sc. Damir Slovenec.<\/p>\n

Rad je dostupan na poveznici: https:\/\/link.springer.com\/article\/10.1007\/s10347-023-00674-7<\/em><\/a><\/p>\n

<\/em><\/a><\/o:p><\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVIEvolution of eastern passive margin of Adria recorded in shallow to deep\u2011water successions of the transition zone between the Alps and the Dinarides (Ivan\u0161\u010dica Mt., NW Croatia)U znanstvenom \u010dasopisu Facies objavljen je znanstveni rad pod naslovom Evolution of eastern passive margin of Adria recorded in shallow to deep\u2011water successions of the transition zone […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-42624","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/42624","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/comments?post=42624"}],"version-history":[{"count":2,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/42624\/revisions"}],"predecessor-version":[{"id":42628,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/42624\/revisions\/42628"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=42624"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}